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Data from: Nikuradse and Shields: turbulent roughness controls shear stress at incipient sediment transport

dc.contributor.authorLouge, Michel Y.
dc.contributor.authorValance, Alexandre
dc.date.accessioned2024-05-31T21:01:51Z
dc.date.available2024-05-31T21:01:51Z
dc.date.issued2024-05-31
dc.description.abstractThis collection contains supporting information for M. Y. Louge, A. Valance, Nikuradse and Shields: turbulent roughness controls shear stress at incipient sediment transport, J. Geophys. Res. Earth Surface (2024). The Nikuradse (1933) data of Darcy friction for turbulent flow in roughened pipe and shear stress measurements at incipient transport from Shields (1936) and later authors indicate that the threshold dimensionless shear stress Sh for entrainment of cohesionless sediment of diameter d is proportional to the 'turbulent roughness' z0 in the core of the boundary layer on a flat surface, Sh = (2.28+/-0.18) (rho/rhos)^(1/3) z0/d, where rhos and rho are material densities of solid and fluid in the range 2.6 < (rhos/rho) < 1.3 10^6. This expression is valid when the boundary layer is fully turbulent for Reynolds numbers 0.63 < Re* < 1100 based on shear velocity and d. Such insight suggests that turbulent roughness governs the entrainment of particles from a planar sediment bed, whether Newtonian liquid or gas continua are involved. It also provides a new interpretation of the ratio z0/d at incipient transport, not as a geometrical aspect ratio, but rather as friction that the turbulent flow must exert to lift sediment from the surface.
dc.description.sponsorshipThis research was supported in part by the National Science Foundation under Grant No. NSF PHY-1748958, which allowed the authors to attend a program at the Kavli Institute for Theoretical Physics, and by the ISblue project, Interdisciplinary Graduate School for the Blue Planet (ANR-17-EURE-0015) that fostered related discussions on dune modeling. A.V. acknowledges the support of the French Research National Agency through project ANR-21-CE30-0066.
dc.identifier.doihttps://doi.org/10.7298/jmnv-fv32
dc.identifier.urihttps://hdl.handle.net/1813/115246
dc.rightsCC0 1.0 Universalen
dc.rights.urihttp://creativecommons.org/publicdomain/zero/1.0/
dc.subjectsedimentology
dc.subjectaeolian transport
dc.subjectsediment transport
dc.titleData from: Nikuradse and Shields: turbulent roughness controls shear stress at incipient sediment transport
dc.typedataset

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